lecture 17
DESCRIPTION
Lecture 17. Tectonic-scale Climate Change. Greenhouse / Icehouse Earth (Part II, p. 84-85; Ch. 4, p. 86-91). Geologic Time Scale. No ice sheets on land. Ice sheets on land. *. *. *. *. *. *. Ice House. Tectonic-scale Climate Change (Ch. 5, p. 103-112). Hundreds of millions of years. - PowerPoint PPT PresentationTRANSCRIPT
Lecture 17Lecture 17
Tectonic-scale Climate Change
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* Ice House
Greenhouse/Icehouse Earth (Part II, p. 84-85; Ch. 4, p. 86-91)
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Geologic Time ScaleNo ice sheets on land Ice sheets on land
Tectonic-scale Climate Change (Ch. 5, p. 103-112)Tectonic-scale Climate Change (Ch. 5, p. 103-112)
Plate tectonics and drift Plate tectonics and drift concentratedconcentrated continents at continents at higher latitudeshigher latitudes allowed for allowed for more ice covermore ice cover, which reflected more sunlight and , which reflected more sunlight and created a positive feedback to cause created a positive feedback to cause greater coolinggreater cooling..
Hundreds of millions of yearsHundreds of millions of years
Seafloor spreading leads to increased Seafloor spreading leads to increased periods of periods of volcanic degassing of COvolcanic degassing of CO22, , which causes warming.which causes warming.
Higher temperaturesHigher temperatures leads to leads to increased increased weatheringweathering, which will , which will remove COremove CO22 from the atmosphere and reverse from the atmosphere and reverse warming in warming in a negative feedback loopa negative feedback loop..
Tectonic-scale Carbon Dioxide Fluctuations Tectonic-scale Carbon Dioxide Fluctuations (p. 91-99; p. 103-(p. 91-99; p. 103-121)121)
Earth’s Climate History in the Last 550 Myr1. Over the past 550
Myr, three Icehouse periods (430, 325-240, 35-0 Myr ago).
2. For most of the last 550 Myr or the earth’s entire history, the climate was much warmer than today.
3. Tectonic-scale climate change is caused byplate tectonics
Land/ocean positions and sizesOcean floor spreading/CO2 increase Mountain building (uplift) &
weathering / CO2 decrease
Part II p. 82-83; Ch. 4, 5, 6, 7
4. Other causes.
Chemical weathering (chemical breakdown of minerals or rocks)
Carbonic acid
Examples: (Calcite) (calcium ions)Limestone + carbon dioxide + water dissolved ions + bicarbonateCaCO3 + CO2 + H2O Ca2+ + 2HCO3
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The World 100 Myr Ago (p. 129-137)The World 100 Myr Ago (p. 129-137)
Flooding of The Flooding of The ContinentsContinents
Cretaceous Greenhouse Earth
Warm period of dinosaursEvidenceNo record of glaciers or polar ice capsFaunal/floral zone latitudinal shiftIsotopes warmer oceansEnvironments shift with near tropics to the polesOceans/Atmosphere/Land FeaturesSea level 100-200 m higher because of no polar ice capsIntense storms (hurricanes) because of warmer watersStronger hydrologic cycleLess wind because lower T and P gradients globallyMore plants, more flowers; extent of dry land reduced by floodingCausesSun-Earth relationshipLand-sea configuration
More oceans in low latitudeslower albedoMore land in high latitudesmore plants
More CO2 in atmosphere (4-8 x)
100,000 years
18,000 years
230,000 years
1 Million years
3.5 Million years
10 million years6 5 million years
10,000 years
1,000 years
55 million years
PRESEN
T1. The last time atmospheric CO2 concentrations and temperatures were much higher than today was in the age of dinosaurs.2. Agriculture revolution began 10,000 years ago.3. Human population explosion in the past 100 years. Today: 6 billion
The only mammals living at this time were small rodents.
Sea levels were much higher than today, and Texas
was mostly under water
What about Texas?
Climate change was one important reason that the
dinosaurs disappeared.
Causes: decrease in ocean floor spreading rate; uplift weathering; ocean heat transport through gateways; ice-albedo feedbacks
Ch. 7
Cooling from leaf outline Cooling from ocean isotopes
Decrease in spreading rate
Global Cooling Trend in the Last 55 Myr